Abstract
Fixation of rat parotid with an unbuffered osmium tetroxide solution containing nearly saturated potassium (pyro)antimonate resulted in abundant deposition of cation-antimonate precipatates in acinar cells. Altering the antimonate concentration, including buffers or chelators in the solution or changing the primary fixative resulted in an altered intensity and distribution of the precipitates formed in the tissue, apparently reflecting a degree of selectivity in ion localization. Decreasing the concentration of pyroantimonate to about half-saturation preserved predominantly the less soluble antimonate salts (e.g., Na+, Ca++) and resulted in preferential retention of deposits along the plasmalemma and in mitochondrial "dense bodies," with loss of most cytoplasmic and nuclear precipitates. A similar pattern was seen if fixation with the high concentration antimonate-osmium procedure was followed by a prolonged rinse. Adding phosphate or collidine buffers markedly decreased precipitates in the nuclei and on granular reticulum as well. Phosphate buffer or ehtyleneglycoltetraacetate inhibited in vitro precipitation of calcium and sodium and decreased or abolished plasmalemmal deposits. Glutaraldehyde fixation, either in the presence of antimonate or prior to antimonate-containing osmium tetroxide, abolished heterochromatin deposits. Mitochondrial dense bodies were of two types, one containing precipitate and the other inherently osmiophilic. The latter were also observed in pyrophosphate-osmium controls. Results from in vitro titrations of cations with the various antimonate methods and from neutron activation analyses of fixed tissues supported conclusions drawn from fine structural distribution patterns and were interpreted as follows. In rat parotid acinar cells, deposits in heterochromatin and on granular reticulum probably arose from precipitation in sites of high K+ and H+ as well as--NH3+-rich histones. Plasmalemmal antimonate deposits demonstrated sites of sodium and/or calcium accumulation. Some mitochondrial dense bodies contained Ca++ whereas others were inherently osmiophilic. Large, extracellular deposits were probably predominantly sodium precipitates.